Volcanoes and Earthquakes - KS2

Part of Primary Topic Packs

Geography

What are volcanoes?

Diagram of the inside of a volcano. Magma is inside it and ash is above it.

Volcanoes can look like small mountains or hills.

A volcano is an opening in the Earth’s crust that allows magma, hot ash and gases to escape.

Magma is molten rock - rock that is so hot it has turned into liquid.

When magma reaches the surface of the Earth, it is called lava. Lava comes out of the volcano as a volcanic eruption, along with gases and ash.

Diagram of the inside of a volcano. Magma is inside it and ash is above it.

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What are the different types of volcano?

Mount Etna erupting
Image caption,
Mount Etna erupting

There are two main types of volcano:

  • composite volcanoes are the most common type of volcano. They can have violent eruptions and can grow bigger as layers of thick lava and ash harden on top of each other. Mount Etna in Sicily, Italy, is an example of a composite volcano.

  • shield volcanoes do not have such violent eruptions. These volcanoes tend to have gentle slopes and their runnier lava spreads and hardens over a wider area. Mauna Loa in Hawaii is an example of a shield volcano.

Mount Etna erupting
Image caption,
Mount Etna erupting
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How do volcanic eruptions happen?

Image of Mauna Loa, Hawaii
Image caption,
Mauna Loa in Hawaii

Most volcanic eruptions are caused by pieces of the Earth's crust, called tectonic plates, moving towards each other.

Some volcanoes, like Mauna Loa in Hawaii are caused by hot spots in the Earth’s crust. These do not erupt violently and lava usually flows slowly out of them.

Eruptions from volcanoes can be very dangerous. They can produce:

  • pyroclastic flows - fast moving clouds of hot ash, gas and rock

  • ash clouds - small pieces of rock and glass that can be carried in the air for many kilometres

  • volcanic bombs - large bits of very hot rock blown out of a volcano

Image of Mauna Loa, Hawaii
Image caption,
Mauna Loa in Hawaii
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Can I have a career in volcanoes?

Did you know that you can get paid to research volcanoes?

Chris has built an exciting career as a volcano vlogger and guide for a company called Going to Extremes. He uses photography and film to record and write about his experiences exploring and climbing inside volcanoes for his blog.

He is currently working with drones to map lava lakes. They measure the height and depth of the lakes, and help to identify any potential signs of new eruptions.

Chris loves sharing his passion for volcanoes with others, helping them witness science in action first-hand, including helping to guide film crews on how to safely access these dangerous environments.

Watch his amazing work in the video below!

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Activity: Make your own erupting volcano!

Have a go at making your own volcano.

Nina from Nina and the Neurons teaches you how to build a volcano using household items.

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Quiz: Volcanoes

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Learn more about volcanoes

Volcanic mountains

2nd Level: People, places and environment

Volcanic mountains

Volcanoes

KS2 History: Geography

Volcanoes
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Earthquakes

What are earthquakes?

Image of Earth opened showing the core, crust and mantle labelled.

The Earth is made up of different layers:

  • the core at the centre, which is mainly metal

  • the mantle, which is mainly rock

  • the crust, which is the part we can see

The crust (together with the upper layer of the mantle) is made up of different pieces, called tectonic plates. These plates fit together like a jigsaw and are moving at a rate of a few centimetres a year, in different directions and at different speeds.

Some plates slide past each other, others move away from each other and some bump into each other.

Sometimes these plates lock together when they meet. This is called a plate boundary or a fault line.

Image of Earth opened showing the core, crust and mantle labelled.
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Watch: How do earthquakes happen?

Diagram of two tectonic plates pushing in opposite directions

As plates move in different directions over long periods of time, friction causes energy to build up.

It becomes so great that the energy is released, which creates a shock wave - an earthquake.

If an earthquake is beneath the ocean it can create a series of huge waves, called a tsunami.

There are thousands of earthquakes across the world each day. Some are quite minor and can only be detected by specialist equipment. But some earthquakes can destroy cities in minutes. The size of an earthquake is measured using the Richter scale.

In some countries like Japan where earthquakes are relatively common, they build earthquake-resistant buildings that sway with the shock waves rather than fall down.

Diagram of two tectonic plates pushing in opposite directions
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Quiz: Earthquakes

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